T
Tetsuya Komabayashi
Researcher at Tokyo Institute of Technology
Publications - 6
Citations - 766
Tetsuya Komabayashi is an academic researcher from Tokyo Institute of Technology. The author has contributed to research in topics: Transition zone & Phase transition. The author has an hindex of 6, co-authored 6 publications receiving 707 citations.
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Journal ArticleDOI
Experimentally determined postspinel transformation boundary in Mg2SiO4 using MgO as an internal pressure standard and its geophysical implications
Yingwei Fei,J. Van Orman,J. Van Orman,Jie Li,Jie Li,W. van Westrenen,W. van Westrenen,Chrystele Sanloup,Chrystele Sanloup,William G. Minarik,Kei Hirose,Tetsuya Komabayashi,Michael J. Walter,Ken-ichi Funakoshi +13 more
TL;DR: In this article, the postspinel transformation boundary in Mg2SiO4 was determined by combining quench technique with in situ pressure measurements, using multiple internal pressure standards including Au, MgO, and Pt.
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Dehydration and earthquakes in the subducting slab: Empirical link in intermediate and deep seismic zones
TL;DR: In this article, a close link between the depth distribution of subduction-zone earthquakes and dehydration events in the hydrated slab-peridotite is established using a combination of thermodynamic calculation and Schreinemakers analysis on previous experimental data.
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Petrogenetic grid in the system MgO-SiO2-H2O up to 30 GPa, 1600°C: Applications to hydrous peridotite subducting into the Earth's deep interior
TL;DR: In this paper, a semiquantitative petrogenetic grid in the system MgO-SiO2-H2O up to 30 GPa and 1600°C was constructed using Schreinemakers analysis on previous experimental data.
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In situ measurements of the majorite-akimotoite-perovskite phase transition boundaries in MgSiO3
TL;DR: In this paper, the phase boundaries between majorite, akimotoite (ilmenite), and perovskite in MgSiO3 determined by in situ measurements in a multi-anvil apparatus.
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Stability of phase A in antigorite (serpentine) composition determined by in situ X-ray pressure observations
TL;DR: In this paper, the authors determined the low-pressure stability limit of phase A in the Mg-end-member antigorite bulk composition defined as the reaction forsterite+water = phase A+enstatite (water-line or "water-storage line") in a multi-anvil apparatus.